第四纪研究
第四紀研究
제사기연구
2010年
1期
216-223
,共8页
张霞%陈亚宁%黄海龙%陈忠升
張霞%陳亞寧%黃海龍%陳忠升
장하%진아저%황해룡%진충승
趋势分析%灰色拓扑预测%年径流量%小波分析%阿克苏河
趨勢分析%灰色拓撲預測%年徑流量%小波分析%阿剋囌河
추세분석%회색탁복예측%년경류량%소파분석%아극소하
trend analysis%gray topological predicting%annual runoff volume%wavelet analysis%Aksu River
根据阿克苏河流域内出山口水文站1957~2006年的径流实测资料,利用数理统计、Mann-Kendall非参数趋势检验及小波分析等方法对径流年际变化特征进行了分析.研究发现,阿克苏河年径流量具有相对稳定且振荡上升的趋势,年际变化小;径流序列在1993年发生突变,径流量呈现出显著增加趋势,且通过了α=0.05的显著性水平检验;丰、枯水周期变化存在着25a左右的主周期,丰水年发生在20世纪90年代后期,且大量连续出现,最长持续时间达7年,枯水年多以连续2年的形式出现,平水年年数占52%.运用灰色拓扑预测方法对突变前后两个径流时间序列分别进行了模拟和预测,模拟结果的平均相对误差仅为12.06%,且位于同一突变区间的精度达97.7%,预测未来几年阿克苏河年径流量存在上升趋势,但趋势不显著.
根據阿剋囌河流域內齣山口水文站1957~2006年的徑流實測資料,利用數理統計、Mann-Kendall非參數趨勢檢驗及小波分析等方法對徑流年際變化特徵進行瞭分析.研究髮現,阿剋囌河年徑流量具有相對穩定且振盪上升的趨勢,年際變化小;徑流序列在1993年髮生突變,徑流量呈現齣顯著增加趨勢,且通過瞭α=0.05的顯著性水平檢驗;豐、枯水週期變化存在著25a左右的主週期,豐水年髮生在20世紀90年代後期,且大量連續齣現,最長持續時間達7年,枯水年多以連續2年的形式齣現,平水年年數佔52%.運用灰色拓撲預測方法對突變前後兩箇徑流時間序列分彆進行瞭模擬和預測,模擬結果的平均相對誤差僅為12.06%,且位于同一突變區間的精度達97.7%,預測未來幾年阿剋囌河年徑流量存在上升趨勢,但趨勢不顯著.
근거아극소하류역내출산구수문참1957~2006년적경류실측자료,이용수리통계、Mann-Kendall비삼수추세검험급소파분석등방법대경류년제변화특정진행료분석.연구발현,아극소하년경류량구유상대은정차진탕상승적추세,년제변화소;경류서렬재1993년발생돌변,경류량정현출현저증가추세,차통과료α=0.05적현저성수평검험;봉、고수주기변화존재착25a좌우적주주기,봉수년발생재20세기90년대후기,차대량련속출현,최장지속시간체7년,고수년다이련속2년적형식출현,평수년년수점52%.운용회색탁복예측방법대돌변전후량개경류시간서렬분별진행료모의화예측,모의결과적평균상대오차부위12.06%,차위우동일돌변구간적정도체97.7%,예측미래궤년아극소하년경류량존재상승추세,단추세불현저.
The Aksu River is a main tributary of the Tarim River,whose upper branches are in the territory of Kirghizsta,132kin long.The Aksu River is composed the two tributaries of the Tuoshigan River and the Kunmalike River.The Aksu Basin lies in an arid and semi-arid region of China,and it has typical hydrographical characteristics of inland rivers in the northwest of China.According to gauged discharges in the two representative hydrologic stations of the Shaliguilanke and the Xiehela,this paper uses a statistical method,the Kendall non-parameter tendency test and the wavelet analysis to analyze annual distribution and variation characteristics on the basis of the observations of annual runoff from 1957 to 2006.The result shows that the variation coefficient over years is small and relatively stable:C_v is 0.154 and the change range increases by 5.29×10~8m~3/10a.On the one hand,the result reveals there was a sudden change in 1993 in the annual runoff sequence,and after this spot,the amount of runoff volume increased distinctly,which passed significance test (α=0.05).On the other hand,for the alternate time for annual runoff high to low,there is an about 25a main cycle,which was obtained through performing multi-scale transformation of the annual runoff sequence using the wavelet analysis theory.The high runoff year appeared continuously in the late 1990s,with a longest duration of 7 years,while the low runoff year mostly appeared in a cycle of two years.The number of normal runoff year account for 52% of the total years.In order to objectively display this complex wave shape of annual runoff change,this paper introduced the gray topology forecasting method.According to the observations of annual runoff data for 30 years(1957~1986) before the sudden change spot,this paper established a grey topological GM(1,1)model and simulated annual runoff volumes before the sudden spot.The mean relative error of simulated results is very low,only 12.06%.and the fitting accuracy is 97.7% in the sudden change interval.Ultimately,using the observations of annual runoff data of 1987 to 2006 establishes another grey topological GM(1,1)model to predict runoff volume in coming years,the results shows that the increase trend of the Aksu annual runoff volume is not obvious in the next five years.